Why are lakes calm in the morning?

During the early morning hours, the land and the water start out at roughly the same temperature. On a calm morning, a given pressure surface will be at the same height above both the land and water. A few hours later, the sun's energy begins to warm the land more rapidly than the water.



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It's all part of what makes weather, the unequal heating of the Earth's surface. That is why over the next couple of months you will hear us often say, “cooler by the lake.” Then again, as boaters and people who enjoy our beautiful waters know, it is always cooler by the lake.

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Water and homes aren't always a match made in heaven. Living near a body of water often results in added maintenance costs. Rising waters can damage your home, and large bodies of water tend to cause additional wear and tear.

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The middle layer, the thermocline, mixes and turns over throughout the year. It turns over due to climate, nutrient variations, and geologic activity such as earthquakes. However, major lake turnover happens during the fall and spring, when the lake's cold and warm waters mix and readjust.

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Lakes can be affected by pollution from various sources such as agricultural runoff, urban development, and recreational activities. High levels of bacteria, harmful algae blooms, and pollutants in the water can pose health risks to swimmers.

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Lastly, many lakes across the world contain high levels of toxins or bacteria, which can be harmful to those who decide to take a dip. Many lakes in America are perfectly safe for swimmers, but these ones can be particularly hazardous and might warrant a second thought before plunging beneath the surface.

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One other thing to be aware of if you're swimming in a freshwater lake, especially in warmer climates: The Centers for Disease Control and Prevention says that swimmers in freshwater lakes should assume brain-eating amoeba are present, although actual cases of infection are extremely rare.

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Three distinct layers develop: The top layer stays warm at around 65–75 degrees F (18.8–24.5 degrees C). The middle layer drops dramatically, usually to 45–65 degrees F (7.4–18.8 degrees C). The bottom layer is the coldest, staying at around 39–45 degrees F (4.0–7.4 degrees C).

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Lakes have layers Water temperatures also play a role in water density. Warm water is less dense meaning it is lighter and stays toward the top of the lake. The colder, heavier water is found at the bottom.

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